Crystal bending in triple-Laue X-ray interferometry. Part I. Theory

Previous studies suggested that the silicon lattice spacing measured by X-ray interferometry might refer to the crystal surface. To confirm this result and to support experimental investigations of the matter, this paper gives a comprehensive analytical model of the operation of a triple-Laue interferometer having one of the splitting and recombining crystals bent.

When the crystal recombining the interfering X-rays (the analyser) is separated, the interference signal is sensitive to movements orthogonal to the diffracting lattice planes. Since a displacement by one plane creates a 2 phase shift, such an interferometer allowed measurement of the lattice parameter of 28 Si with parts per billion accuracy (Massa et al., 2011(Massa et al., , 2015. This result led to the determination of the Avogadro constant (Fujii et al., 2018), the realization of the kilogram by counting atoms (Massa et al., 2020b) and the redefinition of the international system of units (SI) (Wiersma & Mana, 2021).
To realize the kilogram, an essential assumption is that the measured lattice spacing is the bulk value of the unstrained analyser (a blade, typically 1 mm thick). However, surface relaxation, reconstruction and oxidation might cause lattice strains (Melis et al., 2015(Melis et al., , 2016Massa et al., 2020a). Furthermore, analytical and numerical studies of the X-ray propagation in a bent crystal (e.g. because of a difference between the surface stresses of the two surfaces) suggest that the measured lattice spacing might refer to the surface rather than to the bulk (Mana et al., 2004a,b;Apolloni et al., 2008).
To confirm the results of these studies and to support experimental tests of this prediction by phase-contrast topography, we give an analytical model of the operation of a triple-Laue interferometer having, one at a time, the splitter, mirror and analyser crystals cylindrically bent. Our interest is in the phase of the diffracted waves, rather than the intensity profile arising when using bent crystals e.g. to focus X-rays or as analysers for X-ray spectroscopy (Nesterets & Wilkins, 2008;Kaganer et al., 2020;Qi et al., 2021;Guigay & Sanchez del Rio, 2022). This paper is organized as follows. The interferometer operation is outlined in Section 2. Sections 3 and 4 deal with the strain field in a cylindrically bent crystal, the reciprocal vector of the strained lattice and the description of the wavefields in perfect crystals as a two-state quantum system. In Section 5, we solve the Takagi-Taupin equations for X-ray propagation in a bent (symmetrically cut) crystal slab. The propagation in free space is examined in Section 6. Sections 7 and 8 deal with the wavefields leaving a bent crystal and a triple-Laue interferometer having the splitting or recombining crystal bent. In the conclusion, we outline predictions that have been verified by the phase-contrast topography of a monolithic interferometer having one of its crystals bent by a thin copper film (Massa et al., 2023).
All the symbolic computations were carried out with the aid of Mathematica (Wolfram Research, 2021a); the relevant notebook is given as supporting information. To view and interact with it, readers need to download the Wolfram Player which is free of charge (Wolfram Research, 2021b). Fig. 1 shows schematically a symmetrically cut triple-Laue (LLL) X-ray interferometer having a bent mirror and operating in coplanar geometry. It also gives the meaning of some of the symbols that we will use. The interferometer consists of three plane-parallel Si crystals, splitter, mirror and analyser, about 1 mm thick and cut in such a way that the diffracting {220} planes are perpendicular to the surfaces. They split and recombine 17 keV X-rays from a conventional Mo source.

Interferometer operation
To measure the spacing of the diffracting planes, the analyser is moved orthogonally to them. Owing to this displacement, the intensity of the forward-transmitted and reflected beams varies sinusoidally, the period being ideally equal to the sought spacing. The measurement result is the ratio between the displacement (measured absolutely via optical interferometry) and the number of X-ray fringes observed.

Strained crystals
We consider, one at a time, the interferometer crystals cylindrically bent about an axis perpendicular to the x-z plane (see Fig. 1) and approximate the x component of the displacement field, uðrÞ, by the hyperbolic paraboloid (Nesterets & Wilkins, 2008;Kaganer et al., 2020) where À 2 is the Gauss curvature and positive values equal downward bendings, as shown in Fig. 1 (Weisstein, 2023), z ¼ z 0 is the neutral plane, and x ¼ x 0 þ s; z ¼ 0 is the bending axis. Before bending, the input surface of the crystal is z = 0 and the output one z = t. Equation (1) follows from the elastic theory of thin (isotropic) plates having thickness t, where z 0 ¼ t=2, but, for the sake of generality, we do not assume z 0 ¼ t=2. The limit z 0 ! 1 with z 0 ¼ " 0 ¼ const. describes a crystal uniformly strained. The limit x 0 ! 1 with x 0 ¼ # 0 ¼ const. describes a crystal uniformly tilted. In general, in the case of thin crystals, (1) is the first-order approximation of any smooth displacement field.
Equation (1) is not strictly valid in the presence of anisotropy, unpaired surface stresses and Dirichlet boundary conditions imposed at the crystal base. Our finite element analyses and experimental verifications are given by Massa et al. (2023). In particular, we observed that a copper film coated on one of the surfaces bends the crystal in such a way that its opposite, naked, surface lies in the neutral, Àz ¼ z ¼ plane.
We introduced the overall crystal displacement s because, in the determination of the Si lattice parameter by a split-crystal interferometer, the analyser is moved along the x axis. In the analysis of this measurement, x 0 is contained in s and omitted from (1). In the phase-contrast topography of a monolithic interferometer, the x position of the X-ray beam is varied step by step. In the analysis of this measurement, x 0 encodes the X-ray beam displacement and s is contained in x 0 and omitted from (1).
Owing to the bending, the diffracting planes are rotated by ðxÞ ¼ @ z u ¼ ðx À x 0 À sÞ and strained by A positive ðxÞ rotates the diffracting planes in the K o direction and a positive strain means a larger diffracting-plane spacing.
The electric susceptibility of the strained crystal (e.g. in Fig.  1, the mirror) is where r is a position vector and g 0 is a reciprocal vector of the unstrained crystals (e.g. in Fig. 1, of the splitter and analyser). By expanding g 0 Á ðr À uÞ in series, we find that g = g 0 À rðg 0 Á uÞ is a reciprocal vector of a locally perfect crystal. Therefore, by using (1), the reciprocal vector of the strained diffracting planes is where h 0 is the reciprocal vector of the diffracting planes of the unstrained crystals and the x axis is directed along Àh 0 . Hence, as shown in Fig. 1, h 0 ¼ ðÀh 0 ; 0Þ. The sign of 0 depends on the sign choice in the exponent of the plane wavefunctions. One can use either expðik Á rÞ or expðÀik Á rÞ. In the former case, 0 is positive, and in the latter case, it is negative.
The AEh phases depend on the choice of the origin of the coordinate system in the unit cell; a translation u 0 changes AEh according to AEh ! AEh expðAEih 0 Á u 0 Þ. We assume that, for the unstrained planes, ðÀx; zÞ ¼ ðx; zÞ, so that h ¼ Àh . Since expðAEiÞ ¼ À1, the sign of AEh can be chosen as either plus or minus.

Crystal fields
We limit this study to crystals that are symmetrically cut and plane parallel. This choice makes the X-ray propagation two dimensional and dependent only on the inward normalẑ z to the crystal surfaces and an x coordinate that we choose opposite the reciprocal vector h 0 ¼ À2x x=d 0 , where d 0 is the spacing of the diffracting planes of the unstrained crystals (Mana & Palmisano, 2004;Sasso et al., 2022).
Owing to the limited spatial coherence of conventional X-ray sources, each incoming photon is in a probabilistic superposition of single-particle states where we used the Dirac bra-ket notation and The j ðzÞi state belongs to the tensor product L 2 ðR 2 Þ V 2 of the L 2 ðR 2 Þ space of the square-integrable two-variable functions and the two-dimensional vector space V 2 . Throughout the paper we use the 2 Â 1 matrix representation of V 2 . Hence, by omitting the exponentials in (3), In (3), the mean electric susceptibility of silicon 0 is set equal to zero in a vacuum.
where ¼ cosðÂ B Þ and ¼ sinðÂ B Þ are direction cosines and Â B is the Bragg angle, are the kinematical wavevectors satisfying the Bragg conditions We will use the subscript n ¼ o; h to label the V 2 basis vectors and the first (plus or minus) sign of AE and Ç applies always to the o state. Also, we consider a coplanar geometry, that is, The representation of the crystal fields as the components of a state vector (Bonse & Graeff, 1977) allows us to use matrix descriptions of optical components. This simplifies the study of the interferometer, the description of which can be built by assembling simpler elements. This approach is a useful alternative to the standard formulation of the dynamical theory of X-ray diffraction and an additional tool for the study of X-ray interferometry.
In this paper, we consider only the propagation of the coherent single-photon state (2). The averaging over their probabilistic superposition can be done by the density matrix formalism, as shown by Sasso et al. (2022).
To solve the Takagi-Taupin equations, we factor n ðx; zÞ as (Mana & Palmisano, 2004) n ðx; zÞ ¼ I n ðx; zÞ n ðx; zÞ; where, by setting x 0 ¼ x À x 0 À s and z 0 ¼ z À z 0 , Therefore, (5) reads (see the supporting information) Now, it is convenient to use the Fourier transform of n ðx; zÞ with respect to the x variable. Hence, n ðp; zÞ expðÀipxÞ dp; which leads to the reciprocal-space representation of the Takagi where ¼ AEh =j AEh j, ¼ z=Á e is the dimensionless propagation distance, is the dimensionless resonance error, and is the Pendellö sung length. Eventually, crystal propagation is given by where, by solving (8) Tðp; zÞ ¼ cos½ð 2 þ 2 Þ 1=2 À Rðp; zÞ=: To complete the analysis, we need the e n ðp; 0Þ components of the initial state, which are obtained via the convolution integral ð e I Ã n I Ã n Ã e n Þðp; 0Þ. Similarly, after propagation through a crystal having thickness t, we can retrieve the e n ðp; tÞ components of the output state via the convolution integral ð e I I n Ã e n Þðp; tÞ. To calculate these convolution integrals, we rewrite (6b) as where we omitted inessential (constant) phases shared by the o and h states and a phase proportional to h 0 x 2 , is the x component of the reciprocal vector gðzÞ, is the resonance error (Authier, 2001) that makes K n À p x x satisfy the Bragg condition at the hitting point x ¼ 0 of the X-rays, and is the resonance error that makes K n þ q zx x satisfy the Bragg condition versus the x component of the reciprocal vector g z . The physical interpretations of p and q z are given in the supporting information.
In (10), the omission of the h 0 x 2 phase simplifies the convolution integrals, which otherwise must be approximated (giving the same result) by the steepest descent method. It is justified by assuming a limited transverse extension of the X-ray beam about x ¼ 0, i.e. h 0 x 2 is assumed negligibly small everywhere n ðx; zÞ 6 ¼ 0.
Note that g z , u z , p and q z are independent of x. When examining the bending effect on the phase-contrast topography of a monolithic interferometer, we set s = 0. Therefore, u z is the displacement field at x = 0, where the X-rays hit the crystal. When studying the bending effect on the measurement of the Si lattice parameter by a split-crystal interferometer, we set x 0 ¼ 0 and u z ¼ 0.
The Fourier transforms of (10) and of its complex conjugate are (see the supporting information) where the g, u and q subscripts 0 and t indicate z ¼ 0 and z ¼ t, t being the crystal thickness. The e o;h ðp; 0Þ components of the initial state are given by the convolution integrals Similarly, the e o;h ðp; tÞ components of the final state are e n ðp; tÞ ¼ ð e I I n Ã e n Þðp; tÞ After ending the transformation chain describing the X-ray propagation through a bent crystal, where is the reciprocal-space representation of the propagator, are, respectively, the averages of the reciprocal vector g 0;t and displacement u 0;t at the input (subscript zero) and output (subscript t) surfaces, and are their half differences. As shown by (11a) and (11b), the Á g s þ h 0 Á u and gs þ h 0 u phases originate in the matching (ensuring the required continuity) of the input and output waves e ðp; 0Þ and e ðp; tÞ with the guided waves inside the crystal, i.e. the eigenmodes of the Hamiltonian of the Takagi-Taupin equations (5). For this reason, they depend on the lattice parameter and displacement fields at the crystal interfaces. In particular, X-ray propagation as given by (13) and (14) does not depend on the crystal displacement and lattice parameter inside the crystal.
It can be easily verified that, in the case of a displaced perfect crystal, i.e. u ¼ s, the scattering matrix (14) reduces to (9a), where the reflection coefficient Rðp; zÞ gets the h 0 s phase. This makes it possible to measure the spacing of the diffracting planes by making the o and h input states interfere.
If the strain is uniform, i.e. u ¼ " xx ðx À x 0 Þ, then Á g;u and p are equal to zero. Therefore, apart from the different Bragg angle encoded by the resonance error AEq t , the scattering matrix (14) reduces again to (9a), where the reflection coefficient gets the h 0 u ¼ h 0 " xx ðx À x 0 Þ phase and the interference of the o and h input states yields a moiré pattern of upright fringes.
Eventually, if the deformation is a tilt of the diffracting planes, i.e. u ¼ # 0 z, then Á g and q t are equal to zero and g ¼ h 0 , Á u ¼ u ¼ # 0 t=2 and p ¼ 0 K z . Therefore, the scattering matrix (14) reduces to that given by Sasso et al. (2022) to account for a tilted crystal.

Free-space propagation
When studying the interferometer operation, the free-space propagation from one crystal to the next must also be considered. It is given by j e ðp; zÞi ¼ Fðp; zÞj e ðp; 0Þi; where the 0 value in (3) must be set to zero and (see the supporting information) The first-order phase AEpz tanðÂ B Þ corresponds to geometric optics. Accordingly, the o and h states propagate in the K o;h directions. Thus, we have o;h ðx; zÞ = o;h ½x Ç z tanðÂ B Þ; z ¼ 0.
In contrast to propagation in crystals, we approximated the free-space propagation up to the order ðp=KÞ 2 , which brings the exp½ip 2 z=ð2K z Þ factor and recovers the n ðx; zÞ spread because of diffraction. This higher-order approximation is necessary to take into account the propagation of the different plane-wave components of the initial state. As we will make clear in the next section, it allows the incoming diverging rays, one of which is scattered in the K o direction and the other in the K h direction, to leave the source from different points.

Laue diffraction
When X-rays, coming from a source at a distance z S in the o or h state, impinge on a cylindrically bent crystal (plane parallel and symmetrically cut) as shown in Fig. 2, the waves leaving the crystal are (see the supporting information) e ho ðp; tÞ ¼ Rðp À p þ q t ; tÞ e o ðp þ q 0 þ q t ; 0Þ Â exp Ài½gs þ h 0 u À px S À 2q t z S tanðÂ B Þ È É ; ð16aÞ e oo ðp; tÞ ¼ Tðp À p À q t ; tÞ e o ðp þ q 0 À q t ; 0Þ if the input state is j e ðp; 0Þi ¼ e o ðp; 0Þjoi, and e oh ðp; tÞ ¼ Rðp À p À q t ; tÞ e h ðp À q 0 À q t ; 0Þ if the input state is j e ðp; 0Þi ¼ e h ðp; 0Þjhi. They are given by (13), where U B ðp; p 0 ; tÞFðp 0 ; z S Þ substitutes for U B ðp; p 0 ; tÞ.
We omitted second-order terms proportional to q 0 q t =K and irrelevant phases shared by the leaving waves, t is the crystal thickness, z S is the source distance, is the separation at the source of the rays that leave the crystal in the K o;h þ px x directions (see Fig. 2), g t and u t are, respectively, the reciprocal vector and displacement on the crystal research papers J. Appl. Cryst. (2023). 56, 707-715 exit surface and on the axis of the X-ray beam, and q 0 and q t are the additional resonance errors on the crystal input and exit surfaces due to the crystal strain.
The 2q t z S tanðÂ B Þ phase difference between the forwardtransmitted and reflected waves originates in the free-space propagation of the rays exiting the crystal in the K o;h þ px x directions. In fact, they leave the source with different resonance errors, AEq t (see Fig. 2), and, thus, propagation directions.
The phases AEðÁ g s þ h 0 Á u Þ and AEðgs þ h 0 uÞ that come into the forward-transmitted and reflected waves play an essential role in the interferometer operation. As shown in the next section, according to how they add or subtract, they make the interference signal sensitive to the lattice parameter and displacement fields of one or the other side of the bent crystal.

Triple-Laue interferometer
The X-ray propagation through a triple-Laue interferometer having a bent crystal (the splitter or mirror or analyser) is given by e o1 ðpÞ þ e o2 ðpÞ e h1 ðpÞ þ e h2 ðpÞ where X 1 ðp; p 0 Þ and X 2 ðp; p 0 Þ propagate j e ðp 0 ; 0Þi along the first and second arm of the interferometer, respectively. They are built by concatenating crystal and vacuum propagations.
The interferometer unstrained crystals have parallel and unshifted diffracting planes. Therefore, X-ray propagation is carried out by means of (9a). In contrast, propagation in the bent crystal is carried out by means of (14). Vacuum propagation is given by (15). Eventually, to examine separately the two interferometer arms, we introduce the projectors Free-space propagation leads to the separation of the o and h states, leaving the interferometer in two spatially localized states, whose i ¼ 1; 2 components overlap and interfere. In the following subsections, we give the expressions of X 1;2 ðp; p 0 Þ and e ni ðpÞ when the bent crystal is the splitter, mirror or analyser. In the e ni ðpÞ expressions, we neglect inessential phase terms shared by the interfering beams. The detailed calculations are given in the supporting information.

Splitter
When the bent crystal is the splitter, X-ray propagation along the two interferometer arms is given by Fig . 1 gives the meaning of the symbols related to the interferometer geometry (crystal thicknesses and spacing, source and detector distances) that are used here and in the following subsections. The interfering waves reaching the detector are where z S is the source distance from the splitter, is the separation at the source of the rays interfering collinearly, g t S and u t S are, respectively, the reciprocal vector and displacement field on the splitter exit surface, and q 0 and q t S are evaluated on the splitter entrance (subscript 0) and exit  Laue diffraction by a bent crystal. h 0 , reciprocal vector of the unstrained crystal; K o;h , diffracted kinematical wavevectors satisfying the Bragg law for the unstrained crystal; red and blue lines, incoming rays leaving the crystal in the K o (red) and K h (blue) directions; black lines, rays incoming in the K o;h directions; q 0 and q t , resonance errors that make K o;h AE q 0x x and K o;h AE q tx x satisfy the Bragg condition versus the g 0;t components of the reciprocal vectors at the input (subscript 0) and output (subscript t) surfaces, respectively; z S , source distance from the crystal; t, crystal thickness.
(subscript t S ) surfaces. As regards u t S , it is evaluated on the axis of the X-ray beam.
Here and in the next subsections, we leave out the phase terms shared by the interfering wave pairs e o1 ðpÞ and e o2 ðpÞ (o state) and e h1 ðpÞ and e h2 ðpÞ (h state). In addition, we assign the phase difference between the interfering waves to the wave reflected by the analyser, i.e. to e o1 ðpÞ (o state) and e h2 ðpÞ (h state), respectively. The phases of the e o1 ðpÞ and e h2 ðpÞ waves leaving the interferometer originate travelling fringes and moiré interference patterns that encode the diffracting-plane spacing d ¼ 2=g t S and displacement field uðx; t S Þ of the splitter inner surface z ¼ t S . In fact, according to equations (16a)-(16d), the waves travelling along the i ¼ 1; 2 arms acquire, when crossing the splitter, the Á g s þ h 0 Á u and Àðgs þ h 0 uÞ phases, respectively, whose difference is g t S s þ h 0 u t S .

Mirror
When the bent crystal is the mirror, X-ray propagation is given by The detected waves are where z S is the source distance from the mirror, x S ¼ 2qðz S þ z M Þ=K z is the separation at the source of the rays interfering collinearly, are, respectively, the means of the reciprocal vector and resonance error at the input (subscript 0) and output (subscript t M ) surfaces of the mirror, and q 0 and q t M are evaluated on the mirror entrance and exit surfaces. As regards it is the average of the mean displacements u 1;2 calculated along the first (subscript 1) and second (subscript 2) X-ray paths and on the beam axes. Since p depends on the x coordinate along the mirror, the subscript i in p i indicates the mirror crossing of the i ¼ 1; 2 arms. The phases of the e o1 ðpÞ and e h2 ðpÞ waves leaving the interferometer originate travelling fringes and moiré interference patterns that encode the means d ¼ 2=g and uðxÞ of the diffractingplane spacing and displacement field, respectively, of the mirror input and output surfaces. In fact, according to equations (16a)-(16d), the interfering waves, when crossing the mirror, acquire phases having identical gs þ h 0 u magnitude, but opposite signs.

Analyser
When the bent crystal is the analyser, the X-ray propagation is given by The interfering waves are where z S is the source distance from the analyser, is the separation at the source of the rays interfering collinearly, g 0 and u 0 are the reciprocal vector and displacement field, respectively, on the input surface of the analyser, and q 0 and q t A are evaluated on the input (subscript 0) and output (subscript t A ) surfaces of the analyser. As regards u 0 , it is evaluated on the axis of the X-ray beam. The phases of the e o1 ðpÞ and e h2 ðpÞ waves leaving the interferometer originate travelling fringes and moiré interference patterns that encode the diffracting-plane spacing d ¼ 2=g 0 and displacement field uðx; t 0 Þ of the analyser inner surface z ¼ 0. In fact, according to equations (16a)-(16d), the waves travelling along the i ¼ 1; 2 arms acquire, when crossing the analyser, the AEðgs þ h 0 uÞ and AEðÁ g s þ h 0 Á u Þ phases, respectively, where the plus (minus) sign applies to the leaving o ðhÞ state. The phase difference is g 0 s þ h 0 u 0 .

Conclusions
The terms g t S s (if the displaced crystal is the splitter), 2gs (if the displaced crystal is the mirror) and g 0 s (if the displaced crystal is the analyser) in the phase difference of the waves travelling along the first and second arms [see (18), (21) and (24)] make it possible to measure the diffracting-plane spacing. In the case of a displaced mirror, the period of the travelling fringes is half the spacing of the diffracting planes.
Our analysis of the interferometer operation confirms that, in the case of a bent analyser, the sought spacing is measured on the input surface. In fact, in equations (24), the observed phase difference is g 0 s, where g 0 is the x component of the reciprocal vector at the input surface of the analyser. Supported by this result, we surmise that, if the measurement is repeated after flipping the analyser, a difference appears whenever the analyser is (smoothly) strained. These measurement repetitions were used to test the analyser's perfection and corroborate the measurement results (Massa et al., 2011(Massa et al., , 2015. The phase differences h 0 u t S (splitter), 2h 0 u (mirror) and h 0 u 0 (analyser) [see (18), (21) and (24)] are proportional to the displacement fields of the output surface of the splitter, u t S , the input surface of the analyser, u 0 , and the mean u of the displacement fields of the two mirror surfaces. They made it possible to perform experimental tests of our results by the phase-contrast topography of a monolithic interferometer having the splitter or analyser bent by a Cu coating of one of its sides (Massa et al., 2023). We predict that the interferogram is insensitive to what surface (input or output) of the mirror is coated. In contrast, we predict that it is sensitive to which surface (input or output) of the splitter or analyser is coated.
In equations (18), (21) and (24), the arguments of the reciprocal-space representations of the input wavefield e in show that the rays interfering collinearly, i.e. having the same resonance error p when they leave the interferometer, exit the source with different resonance errors, AEq t S (if the bent crystal is the splitter), AEðq 0 þ q t M Þ (if the bent crystal is the mirror) or AEq 0 (if the bent crystal is the analyser). This is the same as saying that they leave the source at different angles. This difference implies two additional terms in the phase difference between the interfering waves.
The first, px S , encodes, via the time-shifting property of the Fourier transform, the fact that the rays interfering collinearly start from different points, spaced by x S . This raises questions about the effect of the source coherence and suggests that a density matrix formalism is needed to describe the interferometer operation (Sasso et al., 2022).
The second, 2q t S z S tanðÂ B Þ (if the bent crystal is the splitter), 2qz S tanðÂ B Þ (if the bent crystal is the mirror) or 2q o z S tanðÂ B Þ (if the bent crystal is the analyser), encodes the different free-space propagation from the source to the interferometer of the rays interfering collinearly. This difference is equal to zero in a perfect interferometer and we surmise it occurs whenever the crystals are (smoothly) strained. Since it makes the interference fringes sensitive to the source distance, a test of the interferometer sensitivity to it might additionally prove (or disprove) the crystals' perfection and, if insensitive, certify the measured values of the diffracting-plane spacing.
Bending causes misalignment of the interferometer splitting and recombining crystals. Firstly, the misalignment stems from the difference between the lattice spacings of the strained and unstrained crystals. This difference is revealed via the q 0 and q t terms in the arguments of the reflection and transmission coefficients. It is independent of the crystal translation and X-ray incidence point -which, in (1), are encoded by the s and x 0 parameters -and originates a meaningless constant contribution to the fringe phase.
Secondly, the misalignment stems from the shear strain ðxÞ of the bent crystal. It is seen in the p term in the argument of the reflection and transmission coefficients, which now depend on the X-ray incidence point. When scanning the X-ray incidence point, this misalignment mimics a continuous rotation of the crystal and it is equivalent to misalignments investigated by Mana & Vittone (1997a,b) and Sasso et al. (2022). The implied phase changes are very small in all practical cases.
APPENDIX A List of the main symbolŝ x x, normal to the diffracting plane. z z, normal to the crystal surface. h 0 ¼ À2x x=d 0 , reciprocal vector (unstrained crystal). d 0 , diffracting-plane spacing (unstrained). ¼ z=Á e , dimensionless propagation distance. t S ; t M ; t A , crystal thicknesses. z S ; z D , source and detector distances. x S , start separation of the rays interfering collinearly. sx x, crystal displacement. h 0 , reciprocal vector (unstrained crystals). g z ; g 0 ; g t , reciprocal vectors (strained crystal, x components).